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- All the exsolution lamellae are brown spinel. 蚀变辉长岩中的斜方辉石已经完全蛇纹石化（保留了斜方辉石假象），斜长石完全被水钙铝榴石交代（保留斜长石假象），但单斜辉石保存完好，且发育由尖晶石叶片（棒）构成的出溶结构。
- GU Lian-xing, Vokes F M.Annealing and coarsening of monoclinic exsolution lamella in pyrrhotite in some nickel-copper ores from Norway[J].Acta Mineralogica Sinaca, 1997, (1) :17 - 23. [3]顾连兴;Vokes F M.;挪威某些铜镍矿石中单斜磁黄铁矿出溶体的退火和粗化[J]
- ANNEALING AND COARSENING OF MONOCLINIC EXSOLUTION LAMELLA IN PYRRHOTITE IN SOME NICKEL-COPPER ORES FROM NORWAY 挪威某些铜镍矿石中单斜磁黄铁矿出溶体的退火和粗化
- exsolution lamellae 出溶层
- exsolution lamella e 出溶层
- Having, composed of, or arranged in lamellae. 薄片的有薄片的、由薄片组成的或按薄片排列的
- Histology reveals cornoid lamellae. 组织病理学特征为角样板层。
- Having the form of a thin plate or lamella. 薄片形的有薄片或鳃瓣状形体的。
- There is not lamella in the ingot. 钢锭没有明显的片层状组织。
- The spinel lamellae (or leafs) are parallel to each other. 棕褐色的尖晶石出溶棒（或叶片）一般完全平行，个别情况下发现两组近于直交的尖晶石出溶棒。
- The sheetlike layers of the thylakoids are called lamellae. 类囊体上的层片叫做片层。
- These lamellae are made up of collagenous fibers and inorganic salt matrix. 这些骨板由胶原纤维和无机盐组成。
- The spores are produced on small teeth or lamellae rather than gills. 孢子都是由子实体的小齿或小孔中产生而不是在菌褶上产生。
- PEG entered the lamellae by replacing part of the inter-lamellar water. PEG通过转换部分层间水进入蒙脱石层间通道内;
- Twin lamellae will be deformed differently when rolling in different direction. 随轧制方向不同，孪晶在形变中的行为也不同。
- With help of this relation, the duration of exsolution and the change rate of mineralizati... 推导了出溶物厚度与过饱和度、生长温度及生长时间的关系；
- The internal lamellae originate from an invagination of the inner of double membrances that surround the plastid. 片层起源于围着质体双层膜的内膜向内折伸。
- Both clinopyroxene and orthopyroxene show exsolution texture.The exsolution rods generally are parallel each other no matter they are straight or curved. 单斜辉石和斜方辉石均发育出溶结构，出溶条纹或者平直或者发生舒缓的弯曲变形（即便是在发生弯曲的情况下也是完全平行的）。
- Tsumoite in the Dashuigou tellurium deposit shows features of both ubiquitous metasomatism and exsolution by its occurrence and graphic-myrmekitic textures it contains. 大水沟楚碲铋矿的产状及其文像矿物形态既有普遍的“交代”现象，也有明显的“出溶”特征。
- The calcite twin lamellae method can be used widely because calcite veins widely develop in faults. 由于方解石脉双晶纹发育的广泛性,使之具有推广价值。
